Abstract

The effects of confining pressure, relative density and sample preparation methods on the shearing strength of Chlef sand were studied in this article. For this purpose, the results of drained and undrained monotonic triaxial compression tests performed on samples with initial density of 0.29 and 0.80 under initial confining pressures ranged from 50 to 200 kPa are presented. The specimens were prepared by two depositional methods namely dry funnel pluviation and wet deposition. It was found that there was a marked difference in the undrained behavior even though the density and stress conditions were identical. The conclusion was that the soil fabric was responsible for this result. The results indicated also that at low confining pressures, the specimens reconstituted by the wet deposition method exhibited complete static liquefaction (zero effective confining pressure and zero stress difference). As confining pressures and densities were increased, the effective stress paths indicated increasing resistance to liquefaction by showing increasing dilatant tendencies. The same trends were observed in drained tests results in the form of an increase in the volumetric strain and the rapid transition from the contractancy phase to the dilatancy phase.

Highlights

  • During static or cyclic loading, the shaking of the ground may cause saturated cohesionless soils to lose their strength and behave like a liquid

  • As can be seen for the samples reconstituted by the wet deposition method, complete static liquefaction occurred in two tests at the lowest confining pressure (50 kPa) irrespective of sand densities

  • At a confining pressure of 100 kPa the specimens undergo temporary liquefaction characterized by the condition where the undrained stress difference first achieves an initial peak, after which it declines to a minimum value

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Summary

Introduction

During static or cyclic loading, the shaking of the ground may cause saturated cohesionless soils to lose their strength and behave like a liquid. This phenomenon is called soil liquefaction and will cause settlement or tipping of buildings, failure of earth dams, earth structures and slopes. The main shock generated an important inverse fault, about 40 km long, appearing on the surface (AMBRASEYS, 1981). The epicenter of this earthquake was localized in the North East of El-Asnam

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